saponite

sap·o·nite

S0084000 (săp′ə-nīt′)n. A clay mineral that is a hydrous silicate of aluminum and magnesium and occurs in soft amorphous masses in the cavities of certain rocks.

[Latin sāpō, sāpōn-, hair dye; see saponin + -ite.]

saponite

(ˈsæpəˌnaɪt) n (Minerals) a clay mineral consisting of hydrated magnesium aluminium silicate and occurring in metamorphic rocks such as serpentine[C19: from Swedish saponit (a rendering of German Seifenstein soapstone), from Latin sāpō soap]

sap•o•nite

(ˈsæp əˌnaɪt)

n. a clay mineral, hydrous magnesium aluminum silicate, belonging to the montmorillonite group: found as a soft filling in rock cavities. [1840–50; < Swedish saponit < Latin sāpō soap]

Saponite

enUK

saponite

[′sap·ə‚nīt] (mineralogy) A soft, soapy, white or light-buff to bluish or reddish trioctahedral montmorillonitic clay mineral consisting of hydrous magnesium aluminosilicate and occurring in masses in serpentine and basaltic rocks. Also known as bowlingite; mountain soap; piotine; soapstone.

Saponite

a mineral, a phyllosilicate of the montmorillonite group; it has the chemical formula NaMg₃[AlSi₃O₁₀]-(OH)₂•4H₂0. Saponite contains Fe as an isomorphic admixture and, sometimes, Cr, Ni, Zn, Cu, and Li. It crystallizes in the monoclinic system. It is found in earthy, clayey or dense, cryptocrystalline masses. When wet, the deposits are soft and oily to the touch; when dry, they are hard and friable. The color is white, yellowish, or reddish. Dry saponite has a hardness of 2.5 on Mohs’ scale, and its density ranges from 2,240 to 2,300 kg/m³. Saponite is formed during the erosion of magnesium minerals of ultrabasic rocks (serpentinites). It has the properties of bentonites (see alsoBLEACHING CLAYS).,

单词	saponite
释义	saponite enUK sap·o·nite S0084000 (săp′ə-nīt′)n. A clay mineral that is a hydrous silicate of aluminum and magnesium and occurs in soft amorphous masses in the cavities of certain rocks. [Latin sāpō, sāpōn-, hair dye; see saponin + -ite.] saponite (ˈsæpəˌnaɪt) n (Minerals) a clay mineral consisting of hydrated magnesium aluminium silicate and occurring in metamorphic rocks such as serpentine[C19: from Swedish saponit (a rendering of German Seifenstein soapstone), from Latin sāpō soap] sap•o•nite (ˈsæp əˌnaɪt) n. a clay mineral, hydrous magnesium aluminum silicate, belonging to the montmorillonite group: found as a soft filling in rock cavities. [1840–50; < Swedish saponit < Latin sāpō soap] Saponite enUK saponite [′sap·ə‚nīt] (mineralogy) A soft, soapy, white or light-buff to bluish or reddish trioctahedral montmorillonitic clay mineral consisting of hydrous magnesium aluminosilicate and occurring in masses in serpentine and basaltic rocks. Also known as bowlingite; mountain soap; piotine; soapstone. Saponite a mineral, a phyllosilicate of the montmorillonite group; it has the chemical formula NaMg₃[AlSi₃O₁₀]-(OH)₂•4H₂0. Saponite contains Fe as an isomorphic admixture and, sometimes, Cr, Ni, Zn, Cu, and Li. It crystallizes in the monoclinic system. It is found in earthy, clayey or dense, cryptocrystalline masses. When wet, the deposits are soft and oily to the touch; when dry, they are hard and friable. The color is white, yellowish, or reddish. Dry saponite has a hardness of 2.5 on Mohs’ scale, and its density ranges from 2,240 to 2,300 kg/m³. Saponite is formed during the erosion of magnesium minerals of ultrabasic rocks (serpentinites). It has the properties of bentonites (see alsoBLEACHING CLAYS).,
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